The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwate...
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2014
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dataone:http://get.iedadata.org/metadata/iso/600104 2024-10-03T18:45:37+00:00 The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica Foreman, Christine BEGINDATE: 2009-07-01T00:00:00Z ENDDATE: 2014-06-30T00:00:00Z 2014-01-01T00:00:00Z http://get.iedadata.org/metadata/iso/600104 unknown IEDA: US Antarctic Program Data Center Antarctic Organisms and Ecosystems Microbiology Biology Glaciology Antarctica Glaciers/Ice Sheet Biosphere Cryosphere US Antarctic Program Data Center (USAP-DC) Dataset 2014 dataone:urn:node:IEDA_USAP 2024-10-03T18:12:02Z Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls' schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer. Dataset Antarc* Antarctic Antarctica Ice Sheet IEDA: US Antarctic Program Data Center (via DataONE) Antarctic Transantarctic Mountains Cotton Glacier ENVELOPE(161.667,161.667,-77.117,-77.117) |
institution |
Open Polar |
collection |
IEDA: US Antarctic Program Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:IEDA_USAP |
language |
unknown |
topic |
Antarctic Organisms and Ecosystems Microbiology Biology Glaciology Antarctica Glaciers/Ice Sheet Biosphere Cryosphere US Antarctic Program Data Center (USAP-DC) |
spellingShingle |
Antarctic Organisms and Ecosystems Microbiology Biology Glaciology Antarctica Glaciers/Ice Sheet Biosphere Cryosphere US Antarctic Program Data Center (USAP-DC) Foreman, Christine The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
topic_facet |
Antarctic Organisms and Ecosystems Microbiology Biology Glaciology Antarctica Glaciers/Ice Sheet Biosphere Cryosphere US Antarctic Program Data Center (USAP-DC) |
description |
Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls' schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer. |
format |
Dataset |
author |
Foreman, Christine |
author_facet |
Foreman, Christine |
author_sort |
Foreman, Christine |
title |
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
title_short |
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
title_full |
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
title_fullStr |
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
title_full_unstemmed |
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
title_sort |
biogeochemical evolution of dissolved organic matter in a fluvial system on the cotton glacier, antarctica |
publisher |
IEDA: US Antarctic Program Data Center |
publishDate |
2014 |
url |
http://get.iedadata.org/metadata/iso/600104 |
op_coverage |
BEGINDATE: 2009-07-01T00:00:00Z ENDDATE: 2014-06-30T00:00:00Z |
long_lat |
ENVELOPE(161.667,161.667,-77.117,-77.117) |
geographic |
Antarctic Transantarctic Mountains Cotton Glacier |
geographic_facet |
Antarctic Transantarctic Mountains Cotton Glacier |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
_version_ |
1811925627292352512 |